{"pageNumber":"430","pageRowStart":"10725","pageSize":"25","recordCount":10951,"records":[{"id":55238,"text":"ofr4488 - 1944 - Zinc-copper deposits near Moth Bay, Revillagigedo Island, southeastern Alaska","interactions":[{"subject":{"id":55238,"text":"ofr4488 - 1944 - Zinc-copper deposits near Moth Bay, Revillagigedo Island, southeastern Alaska","indexId":"ofr4488","publicationYear":"1944","noYear":false,"title":"Zinc-copper deposits near Moth Bay, Revillagigedo Island, southeastern Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":36062,"text":"b963A - 1949 - Some mineral investigations in southeastern Alaska","indexId":"b963A","publicationYear":"1949","noYear":false,"chapter":"A","title":"Some mineral investigations in southeastern Alaska"},"id":1}],"supersededBy":{"id":36062,"text":"b963A - 1949 - Some mineral investigations in southeastern Alaska","indexId":"b963A","publicationYear":"1949","noYear":false,"title":"Some mineral investigations in southeastern Alaska"},"lastModifiedDate":"2023-05-31T21:47:28.776521","indexId":"ofr4488","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1944","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"44-88","title":"Zinc-copper deposits near Moth Bay, Revillagigedo Island, southeastern Alaska","docAbstract":"<p>Moth Bay is a narrow inlet on the north side of the entrance to Thorne Arm, a large bay near the southern end of Revillagigedo Island, southeastern Alaska (see insert, fig. 1). It is about 16 miles by water southeasterly from Ketchikan, the nearest port. Moth Bay is locally known as Maiden Bay. The zinc-copper deposits are about three-fifths of a mile north of the head of the bay, at altitudes ranging from 250 feet to 500 feet, and are accessible by a good trail from the bay. The deposits are near the southern end of a low northward-trending ridge which rises above a broad, swampy, lake-dotted muskeg. The muskeg is bordered on the east and west by smoothly rounded, densely wooded hills up to 2,300 feet high. Vegetation and glacial till cloak most of the surface and rock exposures are rare. Small timber and fresh water are available. The climate is mild and humid.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr4488","usgsCitation":"Robinson, G.D., 1944, Zinc-copper deposits near Moth Bay, Revillagigedo Island, southeastern Alaska: U.S. Geological Survey Open-File Report 44-88, Report: 10 p.; 3 Plates: 19.23 x 19.25 inches or smaller, https://doi.org/10.3133/ofr4488.","productDescription":"Report: 10 p.; 3 Plates: 19.23 x 19.25 inches or smaller","costCenters":[],"links":[{"id":417620,"rank":5,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1944/0088/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":417598,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1944/0088/figure-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":417596,"rank":2,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1944/0088/figure-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":417597,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1944/0088/figure-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":174787,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1944/0088/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Moth Bay, Revillagigedo Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -131.71567909413847,\n              55.888657346691076\n            ],\n            [\n              -131.71567909413847,\n              55.24989899339019\n            ],\n            [\n              -130.87389861118214,\n              55.24989899339019\n            ],\n            [\n              -130.87389861118214,\n              55.888657346691076\n            ],\n            [\n              -131.71567909413847,\n              55.888657346691076\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d5e4b07f02db5dde60","contributors":{"authors":[{"text":"Robinson, G. D.","contributorId":96669,"corporation":false,"usgs":true,"family":"Robinson","given":"G.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":252986,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55239,"text":"ofr4487 - 1944 - Geology and mineral deposits of Glacier Basin and vicinity, Wrangell district, southeastern Alaska","interactions":[{"subject":{"id":55239,"text":"ofr4487 - 1944 - Geology and mineral deposits of Glacier Basin and vicinity, Wrangell district, southeastern Alaska","indexId":"ofr4487","publicationYear":"1944","noYear":false,"title":"Geology and mineral deposits of Glacier Basin and vicinity, Wrangell district, southeastern Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":34529,"text":"b998B - 1953 - Some zinc-lead deposits of the Wrangell district, Alaska","indexId":"b998B","publicationYear":"1953","noYear":false,"chapter":"B","title":"Some zinc-lead deposits of the Wrangell district, Alaska"},"id":1}],"supersededBy":{"id":34529,"text":"b998B - 1953 - Some zinc-lead deposits of the Wrangell district, Alaska","indexId":"b998B","publicationYear":"1953","noYear":false,"title":"Some zinc-lead deposits of the Wrangell district, Alaska"},"lastModifiedDate":"2025-01-14T19:07:38.168956","indexId":"ofr4487","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1944","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"44-87","title":"Geology and mineral deposits of Glacier Basin and vicinity, Wrangell district, southeastern Alaska","docAbstract":"<p>Glacier Basin is on the mainland of southeastern Alaska about 13 miles east of Wrangell (see fig. 1) and is about 10 miles by trail and by boat across Lake Virginia from tidewater (see fig. 2). A Forest Service trail starts from Eastern Passage a few hundred feet north of the mouth of Mill Creek and loads east to the west end of Lake Virginia distance of about 1 mile. It is about 2 miles across Lake Virginia to the start of a blazed trail, at the southeast end of the lake (see fig. 2), to Glacier Basin. The trail is about 6 1/2 miles long and follows the valley of Glacier Creek. It rises from an altitude of 110 feet at Lake Virginia to an altitude of about 2,000 feet in Glacier Basin. The trail is in very poor condition and travel on it is difficult.</p>","language":"English","doi":"10.3133/ofr4487","usgsCitation":"Gault, H., Rossman, D.L., and Flint, G.W., 1944, Geology and mineral deposits of Glacier Basin and vicinity, Wrangell district, southeastern Alaska: U.S. Geological Survey Open-File Report 44-87, Report: 12 p.; 2 Figures: 16.07 x 10.45 inches and 24.38 x 32.08 inches, https://doi.org/10.3133/ofr4487.","productDescription":"Report: 12 p.; 2 Figures: 16.07 x 10.45 inches and 24.38 x 32.08 inches","costCenters":[],"links":[{"id":466243,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1944/0087/figure-3.pdf","text":"Figure 3","linkFileType":{"id":1,"text":"pdf"}},{"id":466242,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1944/0087/figure-2.pdf","text":"Figure 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,{"id":55241,"text":"ofr4428 - 1944 - Occurrences of scheelite in the Solomon district, Seward Peninsula, Alaska","interactions":[],"lastModifiedDate":"2023-07-10T16:49:31.538263","indexId":"ofr4428","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1944","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"44-28","title":"Occurrences of scheelite in the Solomon district, Seward Peninsula, Alaska","docAbstract":"<p>The scheelite occurrences here reported are on the Solomon River, about 35 miles by road east of Nome, the principal town on the Seward&nbsp; Peninsula, and on and near Big Hurrah Creek, about 5 miles northward by road (see fig. 1).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr4428","usgsCitation":"Coats, R.R., 1944, Occurrences of scheelite in the Solomon district, Seward Peninsula, Alaska: U.S. Geological Survey Open-File Report 44-28, 4 p., https://doi.org/10.3133/ofr4428.","productDescription":"4 p.","costCenters":[],"links":[{"id":174790,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1944/0028/report-thumb.jpg"},{"id":418815,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1944/0028/report.pdf","linkFileType":{"id":2,"text":"txt"}}],"country":"United States","state":"Alaska","otherGeospatial":"Seward Peninsula","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -168.3,\n              64.2\n            ],\n            [\n              -161,\n              64.2\n            ],\n            [\n              -161,\n              66.6\n            ],\n            [\n              -168.3,\n              66.6\n            ],\n            [\n              -168.3,\n              64.2\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f4938","contributors":{"authors":[{"text":"Coats, Robert R.","contributorId":37788,"corporation":false,"usgs":true,"family":"Coats","given":"Robert","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":252991,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":53301,"text":"ofr4425 - 1944 - Graphite deposits on the north side of the Kigluaik Mountains, Seward Peninsula, Alaska","interactions":[],"lastModifiedDate":"2023-07-14T13:55:42.68176","indexId":"ofr4425","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1944","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"44-25","title":"Graphite deposits on the north side of the Kigluaik Mountains, Seward Peninsula, Alaska","docAbstract":"<p>The graphite deposits on the north side of the Kigluaik Mountains have been known for many years, and have yielded a small quantity of flake graphite, but they have been only slightly developed. The author spent 4 days of June 1943 in company with Mr. H. E. Heide, mining engineer of the Bureau of Mines, and Mr. Norman Tweet, part owner of one of the properties. Acknowledgment is due Mr. John Read and the Lomen Commercial Company for many favors rendered in connection with the investigation. The chemical analyses in this report were made by F. S. Grimaldi, of the Geological Survey.</p><p>The deposits were examined many years ago by Harrington 1/ who discussed the general geology and described the developments up to the date of'his examination. Much of the history of the district given below is taken from his report.</p><p>According to Harrington, the first claims were staked in 1900. Two principal groups of claims were worked, those of the Uncle Sam Alaska Mining Syndicate and those of the Alaska Graphite Mining Company.</p><p>Harrington records that the claims of the Alaska Graphite Mining Company were staked in part in 1905 and in part in 1915 or 1916. A production of 35 tons picked from talus was reported for 1907. According to Mertie, 2/ the production in 1916 was about 100 tons, which according to Harrington, was shipped in 1917, together with several tons mined from an open cut in that year.</p><p>In 1912, according to Mertie, shipments totalling 130 tons of graphite were made by the Uncle Sam. Alaska Mining Syndicate, and 300 tons were ready for&nbsp;shipment in 1916. Harrington, who visited the area in 1917, reported that no shipments were made in that year by that company.</p><p>No records of subsequent production have been found. The properties apparently lay dormant until the summer of 1943, when renewed interest was expressed in the restaking of claims.</p><p>Graphite deposits are widespread in the Kigluaik Mountains. 3/ The deposits described in the report have received the most attention because of their relative accessibility. These deposits are about 36 miles northwest of Nome and about 26 miles east of Teller (see fig. 1). The principal deposits are 2 to 3 miles from an arm of the Imuruk Basin, and about 27 miles by salt water from Teller. Most of the Imuruk Basin is shallow and does not exceed a fathom in depth at distances as much as a mile from shore. Arrangements may be made at Teller to charter small boats for the trip to the graphite-bearing area.</p><p>The portion of the area between the Kigluaik Mountains and the Imuruk Basin (see fig. 2) is chiefly a gently-sloping alluvial fan, in which the larger creeks are intrenched from 10 to 30 feet near the mountain front.</p><p>The creek herein called Graphite Creek, the northeasternmost creek shown on figure 2, is about 2 miles southwest of the Cobblestone River. Ruby, Ptarmigan and Trail Creeks transect the mountain front in the order named, proceeding southwestward from Glacier Creep. Farther to the southwest, some of the smaller creeks are unnamed. The creek about 1.4 miles southwest of Trail Creek is herein called Christophosen Creek in order to have a convenient means of reference. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr4425","usgsCitation":"Coats, R.R., 1944, Graphite deposits on the north side of the Kigluaik Mountains, Seward Peninsula, Alaska: U.S. Geological Survey Open-File Report 44-25, 10 p., https://doi.org/10.3133/ofr4425.","productDescription":"10 p.","costCenters":[],"links":[{"id":174511,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1944/0025/report-thumb.jpg"},{"id":87152,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1944/0025/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Seward Peninsula","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -168,\n              61.5\n            ],\n            [\n              -160,\n              61.5\n            ],\n            [\n              -160,\n              66.5\n            ],\n            [\n              -168,\n              66.5\n            ],\n            [\n              -168,\n              61.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db6723a2","contributors":{"authors":[{"text":"Coats, Robert R.","contributorId":37788,"corporation":false,"usgs":true,"family":"Coats","given":"Robert","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":247218,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55258,"text":"ofr4434 - 1944 - The Poor Man iron deposit, Kasaan Peninsula, Prince of Wales Island, southeastern Alaska","interactions":[],"lastModifiedDate":"2025-01-14T19:23:35.96839","indexId":"ofr4434","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1944","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"44-34","title":"The Poor Man iron deposit, Kasaan Peninsula, Prince of Wales Island, southeastern Alaska","docAbstract":"<p>The copper-bearing magnetite deposit, known as the Poor Nan prospect, which is on the Iron King No. 3 claim of James Coleman, is 2 miles northwest of the village of Kasaan (see fig. 1) and 35 miles northwest of Ketchikan, the nearest port. The deposit is within 2,000 feet of tidewater in an area ranging in altitude from 50 feet to 200 feet. Outcrops are confined to stream valleys and to prospect cuts and trenches. Most of the area is covered with a veneer of vegetation, glacial drift, and alluvium. The deposit has been explored by three short adits on the west side, four shafts along the east margin, numerous pits and trenches, and 13 drill holes (see fig. 2)</p>","language":"English","doi":"10.3133/ofr4434","usgsCitation":"Warner, L., and Walton, M.S., 1944, The Poor Man iron deposit, Kasaan Peninsula, Prince of Wales Island, southeastern Alaska: U.S. Geological Survey Open-File Report 44-34, Report: 7 p.; 1 Figure: 15.43 x 19.99 inches, https://doi.org/10.3133/ofr4434.","productDescription":"Report: 7 p.; 1 Figure: 15.43 x 19.99 inches","costCenters":[],"links":[{"id":466246,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1944/0034/figure-2.pdf","text":"Figure 2","linkFileType":{"id":1,"text":"pdf"}},{"id":466245,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1944/0034/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":174068,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1944/0034/report-thumb.jpg"},{"id":111480,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.dggs.dnr.state.ak.us/pubs/id/10422","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alaska","otherGeospatial":"Kasaan Peninsula, Prince of Wales Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -134.95054535968126,\n              56.3154368612646\n            ],\n            [\n              -134.95054535968126,\n              54.50909378372856\n            ],\n            [\n              -130.7812500017913,\n              54.50909378372856\n            ],\n            [\n              -130.7812500017913,\n              56.3154368612646\n            ],\n            [\n              -134.95054535968126,\n              56.3154368612646\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67ad97","contributors":{"authors":[{"text":"Warner, L.A.","contributorId":99611,"corporation":false,"usgs":true,"family":"Warner","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":253024,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walton, M. S. Jr.","contributorId":14040,"corporation":false,"usgs":true,"family":"Walton","given":"M.","suffix":"Jr.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":253023,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":16666,"text":"ofr4475_part2 - 1944 - The Mariposa mine, Terlingua quicksilver district, Brewster County, Texas","interactions":[],"lastModifiedDate":"2024-11-14T21:55:22.909235","indexId":"ofr4475_part2","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1944","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"44-75","title":"The Mariposa mine, Terlingua quicksilver district, Brewster County, Texas","docAbstract":"<p>The Mariposa mine in Brewster County, Tex., ranks second in all-time production of quicksilver in the Terlingua mining district. It is in Section 59, Block G-12, and is about 7 miles by road west of the Terlingua Post Office (see accompanying maps). The nearest railroad shipping point is Alpine, Tex., which. is 93 miles by road to the north. The mine is now controlled by the Esperado Mining Co. of Houston, Tex.</p><p>Since 1895 the Mariposa mine has produced between 20,000 and 30,000 flasks of quicksilver. The major production was before 1911, but the mine was active during the first World War, and again during the period from 1933 to 1942. In February 1944, the Esperado Mining Co, was reworking some of the old dumps and exploring an ore showing in the east wall of the Perry pit.</p><p>The productive ground, a rectangular area roughly 3,500 feet long and 1,000 feet wide, centers about California Hill (see plate 1). The principal subsurface workings, about 3 miles of drifts, stapes, and crosscuts, are under California Hill, but much of the ore was taken from numerous pits, trenches, and shafts northeast and west of the hill. Of the 121 shafts over 20 feet deep, 6 are over 100 feet deep and. 2 of these, No. 5 (or Cruz) shaft and the finite shaft, are 300 or more feet deep. The Contratiro winze (see map of workings) extends 200 feet below the 100 level of the mine. Several thousand feet of drifts and crosscuts extending from the deeper shafts explore the mineralized ground through a vertical range of about 300 feet, but almost all the ore that has been produced came from the uppermost workings.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr4475_part2","usgsCitation":"Yates, R., and Thompson, G.A., 1944, The Mariposa mine, Terlingua quicksilver district, Brewster County, Texas (Part 2): U.S. Geological Survey Open-File Report 44-75, 4 p., https://doi.org/10.3133/ofr4475_part2.","productDescription":"4 p.","costCenters":[],"links":[{"id":150353,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1944/0075part2/report-thumb.jpg"},{"id":464032,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1944/0075part2/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":464072,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1944/0075part2/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":464073,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1944/0075part2/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","county":"Brewster County","otherGeospatial":"Mariposa Mine, Terlingua Quicksilver District","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -103.86388352962939,\n              29.61969641631498\n            ],\n            [\n              -103.86388352962939,\n              29.157655817830786\n            ],\n            [\n              -103.0982860556021,\n              29.157655817830786\n            ],\n            [\n              -103.0982860556021,\n              29.61969641631498\n            ],\n            [\n              -103.86388352962939,\n              29.61969641631498\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","edition":"Part 2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bbca","contributors":{"authors":[{"text":"Yates, Robert G.","contributorId":69525,"corporation":false,"usgs":true,"family":"Yates","given":"Robert G.","affiliations":[],"preferred":false,"id":173249,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thompson, George A.","contributorId":94288,"corporation":false,"usgs":true,"family":"Thompson","given":"George","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":173250,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":557,"text":"wsp952 - 1944 - Surface water supply of the United States, 1942, Part II, South Atlantic slope and eastern Gulf of Mexico basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:07","indexId":"wsp952","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1944","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"952","title":"Surface water supply of the United States, 1942, Part II, South Atlantic slope and eastern Gulf of Mexico basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp952","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1944, Surface water supply of the United States, 1942, Part II, South Atlantic slope and eastern Gulf of Mexico basins: U.S. Geological Survey Water Supply Paper 952, viii, 477 p. ;23 cm., https://doi.org/10.3133/wsp952.","productDescription":"viii, 477 p. ;23 cm.","costCenters":[],"links":[{"id":136812,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0952/report-thumb.jpg"},{"id":25120,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0952/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697333","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527529,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2136,"text":"wsp913 - 1944 - Geology and ground-water resources of the Big Spring area, Texas","interactions":[],"lastModifiedDate":"2016-12-27T16:31:29","indexId":"wsp913","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1944","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"913","title":"Geology and ground-water resources of the Big Spring area, Texas","docAbstract":"<p>This report gives the principal results of an investigation of ground water in the Big Spring area, Texas. Big Spring, the county seat of Howard County, has an estimated population of about 16,000. It is situated on the Texas &amp; Pacific Ry. and United States Highway No. 80 in western Texas, about 280 miles west of Fort Worth and along the boundary between the Edwards Plateau and the High Plains. Immediately south of the city is the bold escarpment of the plateau; to the north, west, and southwest lie the High Plains; and to the east lie the Osage Plains. The Edwards Plateau is capped by resistant limestones of Fredericksburg (Lower Cretaceous) age, which have a maximum thickness of about 160 feet. These limestones are underlain by sandstones of Trinity (basal Lower Cretaceous) age, which range in thickness from 60 to 100 feet and which form the principal water-bearing bed of the area. The High Plains are underlain in most places by a varying thickness of silt, clay, sand, and gravel, chiefly of Tertiary age. The Osage Plains are underlain chiefly by Triassic redbeds, which in general form an uneven floor beneath the Cretaceous and younger formations in the High Plains and Edwards Plateau. Beneath the Triassic redbeds is a great thickness of Permian rocks, which in parts of the area contain thick beds of rock salt. Over a large part of the plateau the Cretaceous rocks appear to be fiat lying but actually dip so as to form a northwestward-trending syncline. However, in places the rocks have slumped to form depressions or sinks, which serve as collecting basins for the water from the Trinity sand. As both Triassic and Cretaceous rocks are involved in the deformations, it is believed that they .may have been formed as a result of the solution and removal of the Permian salt by circulating ground water. Two of these sinks have been well known for several years. One of them, usually called the city park sink, is about 2 miles south of Big Spring, and the other, usually called the section 33 sink, is about 6 miles southeast of the city. These sinks are nearly circular. They have a diameter of about 1 mile, and the maximum displacement of the beds is 200 to 300 feet. They serve as collecting basins for ground water drained from the Surrounding Trinity sand, and wells drilled in them yield as much as 300 gallons a minute, largely from the cracks and crevices in the Fredericksburg limestones. As the Trinity sand is mostly fine-grained, wells outside the sinks seldom yield more than 20 to 30 gallons a minute. For many years the water supply of Big Spring and most of the water used there by the Texas &amp; Pacific Ry. Co. has come from wells in the sinks, supplemented by a relatively small supply pumped from well fields between them. It is estimated that the perennial yield of the sinks and intervening well fields amount to an average of about 450,000 gallons a day. For several years-the pumpage has been much more than that, and in 1937 it amounted to an average of about 1,000,000 gallons a day. A large part of the water has therefore come from storage, and as a result the water table in the sinks, where the draft has been greatest, has declined to lower levels each year. If the water supply needed by the city continues to increase at the normal rate, most of the remaining water will be exhausted from the sinks in a few years if no other supply is provided. Although in some areas, such as sees. 44 and 45, the rocks are slightly deformed, no deep sinks that are comparable with the city park and section 33 sinks were found on the Edwards Plateau. A large amount of water is stored in the Trinity sand in areas on the plateau south of the present well fields, but as the sands are fine only small yields can be obtained from wells in them. Near Lees, about 12 miles southwest of Big .Spring, is a structural depression or sink about 1 mile in diameter, which contains Cretaceous limestone that is probably fractured and which is overlain by Tertiary</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp913","usgsCitation":"Livingston, P.P., and Bennett, R., 1944, Geology and ground-water resources of the Big Spring area, Texas: U.S. Geological Survey Water Supply Paper 913, 113 p., https://doi.org/10.3133/wsp913.","productDescription":"113 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":264384,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0913/plate-06.pdf","size":"9896","linkFileType":{"id":1,"text":"pdf"}},{"id":27736,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0913/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137790,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0913/report-thumb.jpg"},{"id":264385,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0913/plate-13.pdf","size":"3573","linkFileType":{"id":1,"text":"pdf"}},{"id":109960,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24684.htm","linkFileType":{"id":5,"text":"html"},"description":"24684"}],"country":"United States","state":"Texas","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db6855d2","contributors":{"authors":[{"text":"Livingston, Penn Poore","contributorId":79452,"corporation":false,"usgs":true,"family":"Livingston","given":"Penn","email":"","middleInitial":"Poore","affiliations":[],"preferred":false,"id":144721,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bennett, Robert R.","contributorId":20723,"corporation":false,"usgs":true,"family":"Bennett","given":"Robert R.","affiliations":[],"preferred":false,"id":144720,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":16664,"text":"ofr4475_part1 - 1944 - 248 mine, Terlingua quicksilver district, Brewster County, Texas","interactions":[],"lastModifiedDate":"2012-07-17T01:01:41","indexId":"ofr4475_part1","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1944","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"44-75","title":"248 mine, Terlingua quicksilver district, Brewster County, Texas","docAbstract":"The 248 quicksilver mine is in Section 248, Block G-4, 2 miles east of Terlingua and 86 miles by dirt road from Alpine, Tex., the nearest railway shipping point (see accompanying maps). Cinnabar, the quicksilver mineral, was discovered before 1902. By 1934 there were only about 700 feet of subsurface workings, but in recent years the Esperado Mining Co., which has the property under lease, has greatly extended exploratory workings and has built a Herreshoff furnace rated at 40 tons per day. At the present time there are 1 1/3 miles of underground workings and 800 feet of surface trenches.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/ofr4475_part1","usgsCitation":"Yates, R., and Thompson, G.A., 1944, 248 mine, Terlingua quicksilver district, Brewster County, Texas (Part 1): U.S. Geological Survey Open-File Report 44-75, 5 p.; 2 Plates: 108 x 52 cm. and 78 x 52 cm., https://doi.org/10.3133/ofr4475_part1.","productDescription":"5 p.; 2 Plates: 108 x 52 cm. and 78 x 52 cm.","costCenters":[],"links":[{"id":258903,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1944/0075part1/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":258901,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1944/0075part1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":258902,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1944/0075part1/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":260293,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1944/0075part1/report-thumb.jpg"}],"country":"United States","state":"Texas","county":"Brewster","otherGeospatial":"Terlingua Quicksilver District","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.75,29.284166666666668 ], [ -103.75,29.366666666666667 ], [ -103.5,29.366666666666667 ], [ -103.5,29.284166666666668 ], [ -103.75,29.284166666666668 ] ] ] } } ] }","edition":"Part 1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd492ae4b0b290850eeef0","contributors":{"authors":[{"text":"Yates, Robert G.","contributorId":69525,"corporation":false,"usgs":true,"family":"Yates","given":"Robert G.","affiliations":[],"preferred":false,"id":173245,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thompson, George A.","contributorId":94288,"corporation":false,"usgs":true,"family":"Thompson","given":"George","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":173246,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70215116,"text":"70215116 - 1944 - Differences in basin‐characteristics as reflected by precipitation‐runoff relations in San Bernardino and Eastern San Gabriel Mountain drainages","interactions":[],"lastModifiedDate":"2020-10-07T18:42:11.50207","indexId":"70215116","displayToPublicDate":"1944-10-07T13:30:43","publicationYear":"1944","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Differences in basin‐characteristics as reflected by precipitation‐runoff relations in San Bernardino and Eastern San Gabriel Mountain drainages","docAbstract":"<p><span>In interpretation and use of basic hydrological data as basis for planning any public works for conservation or control of water, there is great need for a careful and thorough analysis of the precipitation‐runoff relations. Moreover, when such relations may have been worked out for one particular basin, experience has shown that extreme caution must be used in any attempt to apply these relations to another basin even though superficially the latter may appear to be comparable with respect to physiography, meteorological conditions, and all of the other elements which contributed to the relations established for the first basin.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR025i001p00021","usgsCitation":"Stafford, H., and Troxell, H., 1944, Differences in basin‐characteristics as reflected by precipitation‐runoff relations in San Bernardino and Eastern San Gabriel Mountain drainages: Eos, Transactions, American Geophysical Union, v. 25, no. 1, p. 21-35, https://doi.org/10.1029/TR025i001p00021.","productDescription":"15 p.","startPage":"21","endPage":"35","costCenters":[],"links":[{"id":379189,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Bernardino and Eastern San Gabriel Mountain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.938232421875,\n              33.89321737944089\n            ],\n            [\n              -116.54296874999999,\n              33.89321737944089\n            ],\n            [\n              -116.54296874999999,\n              34.5020297944346\n            ],\n            [\n              -117.938232421875,\n              34.5020297944346\n            ],\n            [\n              -117.938232421875,\n              33.89321737944089\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"25","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Stafford, H.M.","contributorId":36914,"corporation":false,"usgs":true,"family":"Stafford","given":"H.M.","email":"","affiliations":[],"preferred":false,"id":800916,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Troxell, H.C.","contributorId":69124,"corporation":false,"usgs":true,"family":"Troxell","given":"H.C.","email":"","affiliations":[],"preferred":false,"id":800917,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":36230,"text":"b940E - 1943 - Occurrence of manganese in eastern Aroostook County, Maine","interactions":[{"subject":{"id":55389,"text":"ofr4347 - 1943 - Manganese deposits of eastern Aroostook County, Maine","indexId":"ofr4347","publicationYear":"1943","noYear":false,"title":"Manganese deposits of eastern Aroostook County, Maine"},"predicate":"SUPERSEDED_BY","object":{"id":36230,"text":"b940E - 1943 - Occurrence of manganese in eastern Aroostook County, Maine","indexId":"b940E","publicationYear":"1943","noYear":false,"chapter":"E","title":"Occurrence of manganese in eastern Aroostook County, Maine"},"id":1}],"lastModifiedDate":"2015-09-08T09:55:25","indexId":"b940E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1943","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"940","chapter":"E","title":"Occurrence of manganese in eastern Aroostook County, Maine","docAbstract":"<p>Manganiferous rocks are found in two areas in eastern Aroostook County, Maine, one west and northwest of Presque Isle and the other south of Houlton. The manganiferous deposits are sedimentary lenses, up to 150 feet thick and half a mile long, in middle Silurian argilllte. The rocks of both areas are much deformed, but the deformation is less intense and the continuity of the deposits therefore greater in the Presque Isle area than in the Houlton area. The dip of the rocks at most deposits is steep to vertical.</p>\n<p>Below the zone of oxidation the manganese occurs as carbonate and as the silicates braunite and bementite. These minerals are primary constituents of the shales and should continue downward to the limits of the sedimentary units that contain them. One deposit, which has been explored by drill- ing to an average depth of 130 feet, contains about 11 percent of manganese, but most of the deposits probably contain be- tween 6.5 and 9 percent. There are many millions of tons of these manganiferOus shales in the county. Some of the deposits contain 20 percent or more of iron., mostly as hematite and limonite, and magnetite is abundant in the Houlton area.</p>\n<p>In parts of the deposits above the water table about 30 percent of the manganese occurs as a heavy stain of secondary oxides along joints and parting planes. . The manganese oxides partly replace the primary rock minerals for a distance of 1 to 3 millimeters from cracks in the rock. At the one deposit from which drilling data are available, manganese oxides are found on only a few fractures below the water table, which is at a depth of 20 feet, and none were seen in rocks from below 45 feet. It is estimated that there may be over 1,700,000 tons of partly oxidized manganiferous shale in the region.</p>\n<p>Some of the deposits are overlain by a thin zone, probably about a foot thick, that is richer in manganese than the underlying oxidized rocks. At the deposit explored by drill- ing, the average manganese content of the deposit as a whole is 76.4 percent of the average as determined from surface sam- ples. The surface enrichment is believed to have taken place before the last advance of the Pleistocene ice, which may have scraped off the enriched part of many deposits. There are probably less than 100,000 tons of enriched rock in all the scattered deposits of the region.</p>\n<p>There is a very much greater tonnage of low-grade unenriched manganlferous rock in Aroostook County, but it cannot be utilized until methods of extraction have been improved.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/b940E","usgsCitation":"White, W., 1943, Occurrence of manganese in eastern Aroostook County, Maine: U.S. Geological Survey Bulletin 940, iv, 37 p., https://doi.org/10.3133/b940E.","productDescription":"iv, 37 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,{"id":55266,"text":"ofr43100 - 1943 - Caamano Point antimony deposit, Cleveland Peninsula, southeastern Alaska","interactions":[{"subject":{"id":55266,"text":"ofr43100 - 1943 - Caamano Point antimony deposit, Cleveland Peninsula, southeastern Alaska","indexId":"ofr43100","publicationYear":"1943","noYear":false,"title":"Caamano Point antimony deposit, Cleveland Peninsula, southeastern Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":36062,"text":"b963A - 1949 - Some mineral investigations in southeastern Alaska","indexId":"b963A","publicationYear":"1949","noYear":false,"chapter":"A","title":"Some mineral investigations in southeastern Alaska"},"id":1}],"supersededBy":{"id":36062,"text":"b963A - 1949 - Some mineral investigations in southeastern Alaska","indexId":"b963A","publicationYear":"1949","noYear":false,"title":"Some mineral investigations in southeastern Alaska"},"lastModifiedDate":"2025-01-13T22:03:59.222612","indexId":"ofr43100","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1943","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"43-100","title":"Caamano Point antimony deposit, Cleveland Peninsula, southeastern Alaska","docAbstract":"<p>The Caamano Paint antimony deposit was examined during the period August 16 to September 10, 1942 by G. D. Robinson of the Geological Survey, U. S. Department of the Interior. The workings were mapped on a scale of 1 inch to 10 feet, and contoured on an interval of 10 feet. As a field setting for the prospect area, the southern part of the peninsula was mapped on a scale of 2 inches to 1 mile.</p><p>The Caamano Point deposit is near the southern tip of the Cleveland Peninsula, southeastern Alaska, 16 miles by water northwest of Ketchikan, the nearest port (see fig. I). The deposit is one-half mile northwest. of the small bay on the- east side of Caamano Point, at an elevation of 140 feet, and is accessible by a good trail from the bay. The property is reported to be owned by Val Klemm of Ketchikan, who located it in February, 1914.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr43100","usgsCitation":"Robinson, G.D., 1943, Caamano Point antimony deposit, Cleveland Peninsula, southeastern Alaska: U.S. Geological Survey Open-File Report 43-100, 4 p., https://doi.org/10.3133/ofr43100.","productDescription":"4 p.","costCenters":[],"links":[{"id":174154,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1943/0100/report-thumb.jpg"},{"id":111473,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.dggs.dnr.state.ak.us/pubs/id/10413","linkFileType":{"id":5,"text":"html"}},{"id":466120,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1943/0100/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Caamano Point, Cleveland Peninsula","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -141.2771233419932,\n              59.764302208687695\n            ],\n            [\n              -141.2771233419932,\n              54.351823380510865\n            ],\n            [\n              -129.96838168669572,\n              54.351823380510865\n            ],\n            [\n              -129.96838168669572,\n              59.764302208687695\n            ],\n            [\n              -141.2771233419932,\n              59.764302208687695\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f97e5","contributors":{"authors":[{"text":"Robinson, G. D.","contributorId":96669,"corporation":false,"usgs":true,"family":"Robinson","given":"G.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":253045,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55423,"text":"ofr4342 - 1943 - Copper Ridge zinc district, eastern Tennessee","interactions":[],"lastModifiedDate":"2020-07-22T14:27:15.031107","indexId":"ofr4342","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1943","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"43-42","title":"Copper Ridge zinc district, eastern Tennessee","language":"ENGLISH","doi":"10.3133/ofr4342","usgsCitation":"Rodgers, J., Kent, D.F., and Hutchinson, R., 1943, Copper Ridge zinc district, eastern Tennessee: U.S. Geological Survey Open-File Report 43-42, HTML Document; 2 Plates: 54.00 x 41.00 inches and 40.00 x 37.00 inches, https://doi.org/10.3133/ofr4342.","productDescription":"HTML Document; 2 Plates: 54.00 x 41.00 inches and 40.00 x 37.00 inches","costCenters":[],"links":[{"id":184750,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":100385,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1943/0042/plate-1.pdf","size":"9593","linkFileType":{"id":1,"text":"pdf"}},{"id":100386,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1943/0042/plate-2.pdf","size":"11544","linkFileType":{"id":1,"text":"pdf"}},{"id":376573,"rank":4,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_93482.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Tennessee","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.7328,\n              36.0806\n            ],\n            [\n              -82.8303,\n              36.0806\n            ],\n            [\n              -82.8303,\n              36.5983\n            ],\n            [\n              -83.7328,\n              36.5983\n            ],\n            [\n              -83.7328,\n              36.0806\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db6861dc","contributors":{"authors":[{"text":"Rodgers, John","contributorId":74436,"corporation":false,"usgs":true,"family":"Rodgers","given":"John","affiliations":[],"preferred":false,"id":253417,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kent, D. F.","contributorId":48232,"corporation":false,"usgs":true,"family":"Kent","given":"D.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":253415,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hutchinson, R.M.","contributorId":68327,"corporation":false,"usgs":true,"family":"Hutchinson","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":253416,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70206703,"text":"70206703 - 1943 -  Geology of the Cimarron Range, New Mexico","interactions":[],"lastModifiedDate":"2019-11-18T12:49:56","indexId":"70206703","displayToPublicDate":"1943-12-31T12:41:16","publicationYear":"1943","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":" Geology of the Cimarron Range, New Mexico","docAbstract":"<p><span>In north-central New Mexico the rugged Cimarron Range marks the eastern margin of the Southern Rocky Mountains, abruptly rising more than 5000 feet above the adjacent Great Plains. Structurally the range is a northward-plunging anticline with a core of pre-Cambrian crystalline rocks. Faulting along the eastern and western margins of the anticline separates the mountains from the Great Plains and the Moreno Valley. North of Cimarron Canyon the anticline plunges beneath the Tertiary sediments of the Raton Coal Basin. To the south the structure is obscured by the basaltic flows of the Ocaté Mesa. Upturned Paleozoic to Tertiary sedimentary rocks crop out along the eastern and northern margin of the anticlinal uplift. Regional relations are obscured by extensive Tertiary intrusions in the northern portion of the area and by the lava flows to the south. In the valley of Rayado Creek a volcanic plug which fed some of the lava flows has been exposed by erosion. In this region there is evidence for a Mid-Tertiary surface of low relief in the central portion of the mountains, a later lava-capped surface believed to be the equivalent of the Broad Valley Stage, the surface of the Park Plateau, and the Ocate Mesa. Three well-developed gravel-capped Pleistocene pediment surfaces extend steplike from the mountain front into the Great Plains. Both structurally and topographically the Cimarron Range is similar to the Colorado Front Range. An attempt is made to reconstruct the geologic history of the Cimarron Range and to fit it into the broader story of the development of the Southern Rocky Mountains in New Mexico. © 1943 Geological Society of America.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.1130/GSAB-54-891","issn":"00167606","usgsCitation":"Smith , J., and Ray, L., 1943,  Geology of the Cimarron Range, New Mexico: Geological Society of America Bulletin, v. 54, no. 7, p. 891-924, https://doi.org/10.1130/GSAB-54-891.","productDescription":"34 p. 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,{"id":70213024,"text":"70213024 - 1943 - The nickel deposits of Yakobi Island, southeastern Alaska","interactions":[],"lastModifiedDate":"2020-09-08T15:23:27.407521","indexId":"70213024","displayToPublicDate":"1943-09-04T11:55:51","publicationYear":"1943","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"The nickel deposits of Yakobi Island, southeastern Alaska","docAbstract":"<p><span>Some of the large, low‐grade nickel‐copper deposits of Bohemia Basin, Yakobi Island, south‐eastern Alaska, which previously had been mapped and studied by the United States Geological Survey, were explored during parts of 1941 and 1942 by the United States Bureau of Mines. The Gealogical Survey interpreted the geologic features of the deposits as revealed by the work of the Bureau of Mines. The explorations were made largely by diamond‐drilling. The three deposits most extensively tested are arranged around a small valley.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR024i001p00257-1","usgsCitation":"Kennedy, G.C., 1943, The nickel deposits of Yakobi Island, southeastern Alaska: Eos, Transactions, American Geophysical Union, v. 24, no. 10, p. 257-257, https://doi.org/10.1029/TR024i001p00257-1.","productDescription":"1 p.","startPage":"257","endPage":"257","costCenters":[],"links":[{"id":378166,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Bohemia Basin, Yakobi Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -136.40899658203125,\n              57.885657378262394\n            ],\n            [\n              -136.37054443359375,\n              57.93964096150508\n            ],\n            [\n              -136.38015747070312,\n              57.98480801923985\n            ],\n            [\n              -136.33895874023438,\n              58.015372741174964\n            ],\n            [\n              -136.494140625,\n              58.11343987475058\n            ],\n            [\n              -136.5655517578125,\n              58.098928399489154\n            ],\n            [\n              -136.56692504882812,\n              57.9826238262452\n            ],\n            [\n              -136.56417846679688,\n              57.91338881058489\n            ],\n            [\n              -136.45706176757812,\n              57.83817241512891\n            ],\n            [\n              -136.40899658203125,\n              57.885657378262394\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"24","issue":"10","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Kennedy, George C.","contributorId":19201,"corporation":false,"usgs":true,"family":"Kennedy","given":"George","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":797996,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70207266,"text":"70207266 - 1943 - Notes on the early history of water-well drilling in the United States","interactions":[],"lastModifiedDate":"2019-12-15T08:52:28","indexId":"70207266","displayToPublicDate":"1943-03-01T08:49:00","publicationYear":"1943","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Notes on the early history of water-well drilling in the United States","docAbstract":"<p><span>The standard cable-tool drilling rig was invented and developed in drilling salt wells in the West Virginia-Ohio-Pennsylvania region during the twenty years following the successful completion of the first drilled well in 1808 by the Ruffnet brothers at the Great Buffalo Lick near Charleston, West Virginia. Some time previous to 1823, Levi Disbrow studied the drilling methods used in the western salt industry and came east to become the first professional water well driller in the states north of the Potomac River. Possibly the first artesian water well in the United States was constructed in 1820 in Charleston, South Carolina, by sinking an iron pipe through a clay bed. Auger boring for artesian water appears to have been first used in Charleston, South Carolina, in 1823; however, the first successful auger-bored well was not completed in that city until after 1825. The drilling methods and tools were copied from a description of a well bored in London, England. Between 1821 and 1833 auger boring of artesian wells began in the Black Belt of Alabama and possibly in Mississippi. The process of jetting wells, invented in 1884, became the chief method of sinking artesian wells in the Atlantic and Gulf Coastal Plain by the end of the century. The first successful artesian wells in Georgia and Florida were put down during the period 1880-1882. © 1943 Society of Economic Geologists, Inc.</span></p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.38.2.119","issn":"03610128","usgsCitation":"Carlston, C., 1943, Notes on the early history of water-well drilling in the United States: Economic Geology, v. 38, no. 2, p. 119-136, https://doi.org/10.2113/gsecongeo.38.2.119.","productDescription":"18 p. ","startPage":"119","endPage":"136","costCenters":[],"links":[{"id":370272,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"38","issue":"2","noUsgsAuthors":false,"publicationDate":"1943-03-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Carlston, C.W.","contributorId":26062,"corporation":false,"usgs":true,"family":"Carlston","given":"C.W.","affiliations":[],"preferred":false,"id":777494,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70157218,"text":"70157218 - 1942 - Eastern Siberia terrain intelligence","interactions":[],"lastModifiedDate":"2015-10-05T13:51:59","indexId":"70157218","displayToPublicDate":"1995-07-24T17:15:00","publicationYear":"1942","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesNumber":"18","subseriesTitle":"Strategic Engineering Study","title":"Eastern Siberia terrain intelligence","docAbstract":"<p>The following folio of terrain intelligence maps, charts and explanatory tables represent an attempt to bring together available data on natural physical conditions such as will affect military operations in Eastern Siberia. The area covered is the easternmost section of the U.S.S.R.; that is the area east of the Yenisei River. Each map and accompanying table is devoted&middot; to a specialized set of problems; together they cover such subjects as geology, construction materials, mineral fuels, terrain, water supply, rivers and climate. The data is somewhat generalized due to the scale of treatment as well as to the scarcity of basic data. Each of the maps are rated as to reliability according to the reliability scale on the following page. Considerable of the data shown is of an interpretative nature, although precise data from literature was used wherever possible. The maps and tables were compiled&nbsp; by a special group from the United States Geological Survey in cooperation with the Intelligence Branch of the Office, Chief of Engineers, War Department.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70157218","usgsCitation":"U.S. Geological Survey Military Geology Branch, 1942, Eastern Siberia terrain intelligence, 29 p., https://doi.org/10.3133/70157218.","productDescription":"29 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":309569,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70157218.JPG"},{"id":309568,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70157218/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"country":"Russia","otherGeospatial":"Eastern Siberia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              27.773437499999996,\n              49.15296965617039\n            ],\n            [\n              27.773437499999996,\n              73.77577986189993\n            ],\n            [\n              76.2890625,\n              73.77577986189993\n            ],\n            [\n              76.2890625,\n              49.15296965617039\n            ],\n            [\n              27.773437499999996,\n              49.15296965617039\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","publicComments":"Prepared under direction of Chief of Engineers, U.S. Army","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55f7efc6e4b05d6c4e4fa99e","contributors":{"authors":[{"text":"U.S. Geological Survey Military Geology Branch","contributorId":127925,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey Military Geology Branch","id":572295,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":45249,"text":"b900J - 1942 - Subsurface geology and oil and gas resources of Osage County, Oklahoma. Part 10, Burbank and South Burbank oil fields, townships 26 and 27 north, range 5 east, and townships 25 to 27 north, range 6 east","interactions":[{"subject":{"id":45249,"text":"b900J - 1942 - Subsurface geology and oil and gas resources of Osage County, Oklahoma. Part 10, Burbank and South Burbank oil fields, townships 26 and 27 north, range 5 east, and townships 25 to 27 north, range 6 east","indexId":"b900J","publicationYear":"1942","noYear":false,"chapter":"J","title":"Subsurface geology and oil and gas resources of Osage County, Oklahoma. 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,{"id":536,"text":"wsp892 - 1942 - Surface water supply of the United States, 1940, Part II, South Atlantic slope and eastern Gulf of Mexico basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:07","indexId":"wsp892","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1942","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"892","title":"Surface water supply of the United States, 1940, Part II, South Atlantic slope and eastern Gulf of Mexico basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp892","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1942, Surface water supply of the United States, 1940, Part II, South Atlantic slope and eastern Gulf of Mexico basins: U.S. Geological Survey Water Supply Paper 892, viii, 441 p. ;23 cm., https://doi.org/10.3133/wsp892.","productDescription":"viii, 441 p. ;23 cm.","costCenters":[],"links":[{"id":136160,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0892/report-thumb.jpg"},{"id":25099,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0892/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6973fd","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527508,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2964,"text":"wsp889A - 1942 - Water supply of the Dakota sandstone in the Ellendale-Jamestown area, North Dakota, with reference to changes between 1923 and 1938","interactions":[],"lastModifiedDate":"2022-12-19T21:45:26.970185","indexId":"wsp889A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1942","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"889","chapter":"A","title":"Water supply of the Dakota sandstone in the Ellendale-Jamestown area, North Dakota, with reference to changes between 1923 and 1938","docAbstract":"<p>The Dakota sandstone underlies most of North Dakota and South Dakota and considerable parts of nearby States. In most of the area that it occupies it is covered with thick deposits of younger formations, chiefly shale, that confine the water in the sandstone under considerable pressure. Where the topography is favorable, as it is in the Ellendale-Jamestown area in southeastern North Dakota, wells that tap the sandstone flow at the surface.</p><p>The first well in North Dakota to tap the Dakota sandstone was drilled in 1886 in the city of Ellendale. It was started as an 8- or 10-inch hole and was finished at a depth of 1,087 feet with a 3%-inch casing. It flowed 600 to 700 gallons a minute and had a pressure reported by different persons as being from 115 to 175 pounds to the square inch.</p><p>The expense of drilling such large and deep wells discouraged their construction for a time. About 1900, however, the jetting method of drilling was introduced^ and during the following two decades hundreds of farm wells 1 inch to 2 inches in diameter were sunk to the sandstone. The decline in artesian head that resulted from the increased draft on the basin was not apparent at first, but by about 1915 the flow of most wells had decreased noticeably and the flow of a few wells in the western part of the area of flow stopped entirely. It is estimated that by 1923 the artesian head at the western boundary of the area of artesian flow had fallen about 330 feet from its original level.</p><p>In 1916 steps were taken to initiate measures for conserving the artesian water in North Dakota, but it was not until 1921 that the State legislature passed a law providing for the reduction of flow of artesian wells to that which could be used beneficially. The enforcement of the law was placed in the office of the State geologist, and this difficult task was assigned to H. E. Simpson, who directed the work until his death in 1938. Between 1923 and 1928 each artesian well in the Ellendale-Jamestown area was visited and advice was given the owner regarding the flow to which his well should be reduced. Many of the wells were visited again between 1928 and 1935 in order to check on whether the flow had been&nbsp;sufficiently reduced. Through this program much artesian water was conserved and much valuable information was obtained on the discharge from the basin. </p><p>It is estimated that between 1920 and 1923 the artesian head in the western part of the Ellendale-Jamestown area declined at an annual rate of about 4 feet, whereas in 1938 the rate of decline was only about 0.5 foot a year. Between 1915 and 1923 the part of the area of artesian flow in the Edgeley quadrangle was reduced an average of 16.5 square miles a year as a result of the eastward movement of the western boundary of the area. Between 1923 and 1938, however, the average rate of shrinkage of this part of the area of artesian flow was only about 4.5 square miles a year. The perennial recharge to each row of townships in the area of artesian flow has been estimated to be about 500 gallons a minute. In 1923 the flow from wells in T. 129 N., Rs. 50 to 65 W., was about 1,000 gallons a minute, or twice the estimated recharge. In 1938 the flow from wells in this row of townships was about 520 gallons a minute, or only slightly more than the estimated recharge. Thus it appears that a balance is being approached between the withdrawal of water from the basin and the perennial recharge to it.</p><p>It is believed that the water withdrawn from the basin in excess of the perennial recharge has been obtained from storage by the compression of .the sandstone and associated beds of shale due to the increased load placed upon them by the decline in artesian pressure. Calculations made on this theory indicate that the coefficient of storage is about 0.001 that is, about 0.001 cubic foot of water is released from each column of sandstone and shale 1 foot square for each foot of decline in artesian head. Additional computations show that the effect of the large decline in artesian pressure in southeastern North Dakota probably has caused only a few feet of lowering of artesian head at distances of more than 100 miles west of the area of artesian flow.</p><p>The quality of the artesian water is very poor and much of it is unfit for human consumption. Of the 33 analyses included in this report, all show total dissolved solids of more than 2,200 parts per million. Much of the water is salty, and all contains sufficient fluoride to cause mottling of the enamel of the teeth. The temperature of the water from flowing wells ranges from 47° to 69° F.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp889A","usgsCitation":"Wenzel, L.K., and Sand, H.H., 1942, Water supply of the Dakota sandstone in the Ellendale-Jamestown area, North Dakota, with reference to changes between 1923 and 1938: U.S. Geological Survey Water Supply Paper 889, Report: iv, 81 p.; 1 Plate: 25.50 × 39.00 inches, https://doi.org/10.3133/wsp889A.","productDescription":"Report: iv, 81 p.; 1 Plate: 25.50 × 39.00 inches","numberOfPages":"97","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":410741,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24677.htm","linkFileType":{"id":5,"text":"html"}},{"id":139262,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0889a/report-thumb.jpg"},{"id":29693,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0889a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29692,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0889a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Dakota","otherGeospatial":"Ellendale-Jamestown area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -99,\n              47\n            ],\n            [\n              -99,\n              45.936\n            ],\n            [\n              -98,\n              45.936\n            ],\n            [\n              -98,\n              47\n            ],\n            [\n              -99,\n              47\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5effee","contributors":{"authors":[{"text":"Wenzel, Leland Keith","contributorId":38134,"corporation":false,"usgs":true,"family":"Wenzel","given":"Leland","email":"","middleInitial":"Keith","affiliations":[],"preferred":false,"id":146057,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sand, H. H.","contributorId":12026,"corporation":false,"usgs":true,"family":"Sand","given":"H.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":146056,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4621,"text":"wsp922 - 1942 - Surface water supply of the United States, 1941, Part II, South Atlantic slope and eastern Gulf of Mexico basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:40","indexId":"wsp922","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1942","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"922","title":"Surface water supply of the United States, 1941, Part II, South Atlantic slope and eastern Gulf of Mexico basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp922","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1942, Surface water supply of the United States, 1941, Part II, South Atlantic slope and eastern Gulf of Mexico basins: U.S. Geological Survey Water Supply Paper 922, viii, 433 p. ;23 cm., https://doi.org/10.3133/wsp922.","productDescription":"viii, 433 p. ;23 cm.","costCenters":[],"links":[{"id":139221,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0922/report-thumb.jpg"},{"id":31678,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0922/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69744c","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528314,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70206632,"text":"70206632 - 1942 - Reconnaissance survey of the Roberts Mountains, Nevada","interactions":[],"lastModifiedDate":"2024-09-24T18:38:09.426143","indexId":"70206632","displayToPublicDate":"1942-12-01T08:26:06","publicationYear":"1942","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Reconnaissance survey of the Roberts Mountains, Nevada","docAbstract":"<p><span>The Roberts Mountains region, central Nevada, provides an excellent section of Paleozoic rocks ranging from Upper Cambrian to Permian. Major low-angle thrusting is indicated by deformed Ordovician strata resting on Paleozoics of varying age. Overlying a thick breccia zone, the upper thrust plate consists of sandstones, andesitic flows and tuffs, black shales, and bedded cherts (Vinini formation). Ordovician age of the Vinini is established on the basis of graptolite faunules. A belt of Lower to Middle Ordovician graptolitic facies similar to the Vinini formation crosses the Great Basin west of Roberts Mountains. Deposits of roughly the same age in the Roberts Mountains meridian and eastward are dominantly limestone, carrying distinct faunas. Axial planes of overturned folds in the thrust plate dip west, a further indication that the upper thrust plate moved from west to east. Minimum horizontal displacement is 16 miles. The date of thrusting is uncertain, but presumably was later Cretaceous or early Tertiary. Following thrusting, an alaskite stock and rhyolite porphyry plugs were intruded; lava flows and tuffs covered the area in part. Thrust plate and cover of volcanics have been broken into normal fault blocks. The post-thrusting igneous rocks, like volcanic rocks of Utah and New Mexico, are characterized by high potash content.&nbsp;</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/GSAB-53-1675","usgsCitation":"Merriam, C., and Anderson, C., 1942, Reconnaissance survey of the Roberts Mountains, Nevada: Geological Society of America Bulletin, v. 53, no. 12, p. 1675-1727, https://doi.org/10.1130/GSAB-53-1675.","productDescription":"53 p.","startPage":"1675","endPage":"1727","costCenters":[],"links":[{"id":369196,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Roberts Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -116.47304167084806,\n              39.96228576658174\n            ],\n            [\n              -116.47304167084806,\n              39.69688865629308\n            ],\n            [\n              -116.1191336966752,\n              39.69688865629308\n            ],\n            [\n              -116.1191336966752,\n              39.96228576658174\n            ],\n            [\n              -116.47304167084806,\n              39.96228576658174\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"53","issue":"12","edition":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Merriam, C.W.","contributorId":51350,"corporation":false,"usgs":true,"family":"Merriam","given":"C.W.","email":"","affiliations":[],"preferred":false,"id":775272,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, C.A.","contributorId":105277,"corporation":false,"usgs":true,"family":"Anderson","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":775273,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70213112,"text":"70213112 - 1942 - Solution‐phenomena in the Pecos basin in New Mexico","interactions":[],"lastModifiedDate":"2020-09-10T13:22:15.857176","indexId":"70213112","displayToPublicDate":"1942-09-09T12:35:17","publicationYear":"1942","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Solution‐phenomena in the Pecos basin in New Mexico","docAbstract":"<p><span>The drainage‐basin of the Pecos River in New Mexico is a broad asymmetric trough extending from the Sangre de Cristo Mountains southward into Texas (see Fig. 1). It is bounded on the east by the westward facing escarpment of the High Plains and on the west by the crests of the Guadalupe, Sacramento and Sierra Blanca mountains, and a poorly defined divide extending northward through Gallinas Mountain and Pedernal Mountain to Glorieta Mesa. Most of the basin is formed by extensive upland erosion‐surfaces that slope gently toward the river. The valley proper, through much of its length, is relatively narrow and is bounded by steep marginal bluffs, but in some sections, notably between Acme and Lakewood (the Roswell artesian basin) and between Carlsbad and Black River, it is considerably expanded and the lowlands adjoining the river extend from 3 to 16 miles back from the river.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR023i001p00027","usgsCitation":"Morgan, A., 1942, Solution‐phenomena in the Pecos basin in New Mexico: Eos, Transactions, American Geophysical Union, v. 23, no. 1, p. 27-25, https://doi.org/10.1029/TR023i001p00027.","productDescription":"9 p.","startPage":"27","endPage":"25","costCenters":[],"links":[{"id":378278,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Mexico","otherGeospatial":"Pecos River Drainage Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -103.1396484375,\n              35.94243575255426\n            ],\n            [\n              -106.45751953125,\n              36.03133177633187\n            ],\n            [\n              -107.99560546875,\n              35.67514743608467\n            ],\n            [\n              -107.4462890625,\n              33.211116472416855\n            ],\n            [\n              -107.20458984375,\n              32.008075959291055\n            ],\n            [\n              -103.24951171875,\n              32.045332838858506\n            ],\n            [\n              -103.1396484375,\n              35.94243575255426\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"23","issue":"1","edition":"18","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Morgan, Arthur M.","contributorId":59051,"corporation":false,"usgs":true,"family":"Morgan","given":"Arthur M.","affiliations":[],"preferred":false,"id":798436,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70207285,"text":"70207285 - 1942 - Deep‐seated solution in the Meade basin and vicinity, Kansas and Oklahoma","interactions":[],"lastModifiedDate":"2019-12-16T06:30:25","indexId":"70207285","displayToPublicDate":"1942-08-31T06:24:19","publicationYear":"1942","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Deep‐seated solution in the Meade basin and vicinity, Kansas and Oklahoma","docAbstract":"<p><span>During the closing years of the 19th century, Haworth [see 1 and 2 of “References” at end of paper] and Johnson [3] noted the abundant depressions resembling sink‐holes in the Southern High Plains, especially in Meade and Clark counties, Kansas, and Beaver County, Oklahoma. Johnson was of the opinion that all the depressions and basins in this region were due to solution, whereas Haworth [1] believed the Meade artesian basin to be structural, although he held to a solutional origin for the Ashland and Englewood basins, which are a few miles to the east. ©1942. American Geophysical Union. All Rights Reserved.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR023i001p00035","issn":"00028606","usgsCitation":"Frye, K., and Schoff, S., 1942, Deep‐seated solution in the Meade basin and vicinity, Kansas and Oklahoma: Eos, Transactions, American Geophysical Union, v. 23, no. 1, p. 35-39, https://doi.org/10.1029/TR023i001p00035.","productDescription":"5 p. ","startPage":"35","endPage":"39","costCenters":[],"links":[{"id":370292,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States ","state":"Kansas, Oklahoma ","county":"Meade, Clark, Beaver","otherGeospatial":"Meade basin ","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-99.5557,37.4689],[-99.5551,37.3832],[-99.5435,37.3828],[-99.5399,36.9998],[-100.0009,36.9985],[-100.0024,36.9985],[-100.004,36.8538],[-100.0044,36.76],[-100.0045,36.5917],[-100.0044,36.5849],[-100.0038,36.4998],[-100.1458,36.4998],[-100.3204,36.4999],[-100.5459,36.4994],[-100.7022,36.5],[-100.8939,36.4998],[-100.9524,36.4998],[-100.9534,36.8476],[-100.9448,36.8478],[-100.9441,36.9988],[-100.6337,36.9986],[-100.635,37.3881],[-100.6518,37.3878],[-100.652,37.4757],[-100.217,37.4758],[-100.1068,37.4751],[-99.5557,37.4689]]]},\"properties\":{\"name\":\"Clark\",\"state\":\"KS\"}}]}","volume":"23","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Frye, K.C.","contributorId":221248,"corporation":false,"usgs":false,"family":"Frye","given":"K.C.","email":"","affiliations":[],"preferred":false,"id":777540,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schoff, S.L.","contributorId":107365,"corporation":false,"usgs":true,"family":"Schoff","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":777541,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":37965,"text":"37965 - 1942 - Blackbirds and grain crops in the eastern United States","interactions":[],"lastModifiedDate":"2014-07-18T13:23:51","indexId":"37965","displayToPublicDate":"1942-06-01T13:23:13","publicationYear":"1942","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"220","title":"Blackbirds and grain crops in the eastern United States","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Dept. of the Interior","publisherLocation":"Washington, D.C.","usgsCitation":"Kalmbach, E., 1942, Blackbirds and grain crops in the eastern United States: Wildlife Leaflet 220, 5 p.","productDescription":"5 p.","numberOfPages":"5","costCenters":[],"links":[{"id":290473,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4f9fe4b0b290850f2d31","contributors":{"authors":[{"text":"Kalmbach, E.R.","contributorId":21610,"corporation":false,"usgs":true,"family":"Kalmbach","given":"E.R.","email":"","affiliations":[],"preferred":false,"id":218703,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}